The continental shelf is always very wide, extending tens to hundreds of kilometers seaward.
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Q1: The Pacific, Atlantic, Arctic, and Indian Oceans
Q2: The geologic margin of a continent is
Q3: The change from continental crust to oceanic
Q5: The sediment accumulated on continental shelves consists
Q6: Submarine canyons are eroded by turbidity currents.
Q7: An active continental margin forms adjacent a
Q8: Relative to an active margin, the continental
Q9: Relative to an active margin, the continental
Q10: Abyssal plains tend to be most common
Q11: Rifting within continental crust is an important
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